OnSH type of motion due to body forces and due to stress-discontinuity in a semi-infinite viscoelastic medium-Reference-Cited by-同舟云学术

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OnSH type of motion due to body forces and due to stress-discontinuity in a semi-infinite viscoelastic medium

Published:1963-05 Issue:1 Volume:55 Page:42-52
ISSN:0033-4553
Container-title:Geofisica Pura e Applicata
language:en
Short-container-title:Geofisica Pura e Applicata

Author:

Sarker A. K.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF02011214.pdf

Reference7 articles.

1. Cagniard L.:Réflexion et réfraction des ondes séismiques progressives. Paris, 1939.

2. Das Gupta S. C.: Geofis. pura e appl., 32 (1959), 49.

3. Erdelyi, A.:Tables of Integral Transforms, Vol. 1; Mc. Graw Hill, 1954.

4. Garvin W. W.: Proc. Roy. Soc. (A) 234 (1956), 528.

5. Jaeger J. C.:Elasticity, Fracture and Flow. Methuen & Co. Ltd., 1962, pp. 101–103.

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Generation and propagation ofSH-type waves due to stress discontinuity in a linear viscoelastic layered medium;Proceedings Mathematical Sciences;1995-05

2. Propagation ofSH-waves in a heterogeneous visco-elastic layer overlying a homogeneous voigt medium;Pure and Applied Geophysics PAGEOPH;1969

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